Results 91 to 100 of about 5,077 (206)
The age of ulramafic rocks of the Karabash massif (1720-1740 Ma), the minimum age of their protolith (1830 Ma), and the age of formation of rodingites (438.5 ± 15 Ma) and chlorite-carbonate rocks (404.4 ± 8.8 Ma) were determined on the basis of the ...
A. A. Krasnobaev, P. M. Valizer
doaj +2 more sources
Vibrational Spectroscopy of Serpentinite Phase Transformations and Significance of OH Bands
Serpentine group minerals—comprising antigorite, chrysotile, and lizardite—are key indicators of the hydration of ultramafic rocks and the serpentinization process.
Ayşe Didem Kılıç +2 more
doaj +1 more source
Agbaja Plateau is one of the mesas that dotted the topography of north centrally located Bida Basin. Seventeen shale samples from the exposed Maastrichtian Patti Formation at Agbaja Plateau were analyzed using x-ray fluorescence (XRF) and
Olusola Ojo +3 more
doaj +1 more source
The protolith nature of diamondiferous metamorphic rocks of the Kokchetav Massif [PDF]
Vladislav Shatsky +5 more
openaire +1 more source
Zircon Stability Grids in Partial Melts from Different Protoliths [PDF]
Fernando Bea +4 more
openaire +1 more source
Correlation analysis(N.ys).tex
The correlation matrix between the refractive index of terahertz spectra and the content of each element in the ...
Tong Zhang (7879841) +4 more
core +1 more source
Logbadjeck is situated in the northern edge of the Congo Craton, Nyong Series, Cameroon. This paper presents the petrographic and geochemical characteristics of biotite gneiss and amphibolite mined as aggregates and the environmental impact of quarrying ...
Anicet Feudjio Tiabou +5 more
doaj +1 more source
Migmatite-cored gneiss domes in the Himalaya are valuable structures that expose the mid-crust, allowing for the investigation of tectonic and structural processes governing the evolution of the Himalayan orogen.
Ahenda, Mark
core
Metasomatism occurs when fluid interacts with rock to add, or remove, its chemical constituents; these processes form mineral deposits where economic element(s) are concentrated into small volumes of rock.
Shawn Hood (14739418) +2 more
core
TFe elemental content of protolith samples at different depths. Absorption coefficients at different frequencies versus depth.
Tong Zhang (7879841) +8 more
core +1 more source

